Ice rafted debris flux to sediment core FOX12-02R

Fuente: PANGAEA
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Autori principali: Vermassen, Flor, Bjørk, Anders Anker, Sicre, Marie-Alexandrine, Jaeger, John, Wangner, David Johannes, Kjeldsen, Kristian Kjellerup, Siggaard-Andersen, Marie-Louise, Klein, Vincent, Mouginot, Jeremie P, Kjær, Kurt Henrik, Andresen, Camilla S
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2019
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author Vermassen, Flor
Bjørk, Anders Anker
Sicre, Marie-Alexandrine
Jaeger, John
Wangner, David Johannes
Kjeldsen, Kristian Kjellerup
Siggaard-Andersen, Marie-Louise
Klein, Vincent
Mouginot, Jeremie P
Kjær, Kurt Henrik
Andresen, Camilla S
author_facet Vermassen, Flor
Bjørk, Anders Anker
Sicre, Marie-Alexandrine
Jaeger, John
Wangner, David Johannes
Kjeldsen, Kristian Kjellerup
Siggaard-Andersen, Marie-Louise
Klein, Vincent
Mouginot, Jeremie P
Kjær, Kurt Henrik
Andresen, Camilla S
collection Datos científicos de ciencias marinas y ambientales
contents The samples were wet-sieved, separating them into grain-size fractions , (63-150 µm, and >150 µm). For the >150 µm fraction, individual grains that weighed more than 0.01 g were discarded in order to reduce distortion of the grain size signal resulting from the occurrence of singular large grains. Weight percentages of the sand fraction were calculated relatively to the total dry weight. Sediment weight percentages were converted to IRD fluxes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_908230
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Ice rafted debris flux to sediment core FOX12-02R
Vermassen, Flor
Bjørk, Anders Anker
Sicre, Marie-Alexandrine
Jaeger, John
Wangner, David Johannes
Kjeldsen, Kristian Kjellerup
Siggaard-Andersen, Marie-Louise
Klein, Vincent
Mouginot, Jeremie P
Kjær, Kurt Henrik
Andresen, Camilla S
DEPTH, sediment/rock; FOX12-02R; Ice rafted debris, flux; IRD; SEDCO; Sediment corer
The samples were wet-sieved, separating them into grain-size fractions , (63-150 µm, and >150 µm). For the >150 µm fraction, individual grains that weighed more than 0.01 g were discarded in order to reduce distortion of the grain size signal resulting from the occurrence of singular large grains. Weight percentages of the sand fraction were calculated relatively to the total dry weight. Sediment weight percentages were converted to IRD fluxes.
title Ice rafted debris flux to sediment core FOX12-02R
topic DEPTH, sediment/rock; FOX12-02R; Ice rafted debris, flux; IRD; SEDCO; Sediment corer
url https://doi.org/10.1594/PANGAEA.908230